Understanding the three types of supercell thunderstorms. The rear flank downdraft rfd is a key ingredient in tornado formation in supercell thunderstorms. Feb 11, 2009 a rear flank downdraft is cold air on the back side of the storm that rushes down towards the ground and when that cold air hits the cloud base associated with the updraft it quickly erodes them leaving a clear slot. A country journal for gay men everywhere is a readerwritten magazine focused on gay countryliving and alternative lifestyles.
Rear flank downdraft how is rear flank downdraft abbreviated. The rearflank downdraft rfd gust front is indicated by a dashed blue line labeled rfdgf in fig. Some other complex factors beyond the scope of the course also contribute to the formation of the rfd, but the bottom line is that a separate rearflank downdraft exists in supercells. In this paper, in situ surface observations within hook echoes and rfds are analyzed. Jan 15, 2010 rear flank downdrafts have a wellestablished association with hook echoes. The rfd of a supercell is believed to play a large part in tornadogenesis by tightening existing rotation within the surface mesocyclone.
These geometric features are key elements in the formation of tornadoes. A strong downdraft of air on the upwind side of a thunderstorm, usually a supercell, which is separated from the forward flank regions of the storm. The rfd also may wrap around a rotating supercell storm, especially is the storm is tornadic. A lot of times it will create sort of a horse shoe shape in the updraft base.
This supercell drifted eastward very slowly, and was nearly stationary at times. The rear flank downdraft is this part over here, so you can see the downdraft over here. Hook echoes are known to be associated with a commonly observed region of subsiding air in supercells, called the rearflank downdraft. At such close distance to the radar rear flank downdraft rfd inflow air could be recycled and becomes part of the rear flank downdraft. Founded in 1974, the magazine has been edited at various locations and by different communities over the course of its existence. These winds can sound like a freight train and in some cases they can be strong enough to mimic tornado damage. If it is in contact with the ground it is a tornado. Rear flank downdraft meteorology definition,meaning.
The hybrid method estimates high frequency turbulence regeneration in an actual severe storm that has complex thermal conditions in order to alleviate the problem of high frequency component dissipation in meteorological models and generate appropriate. The rear flank downdraft is air from aloft that is transported down to the surface from colliding with the storm. Time lapse video 8x speed of the tornadic supercell west of syracuse, ks on 71516. Evolution of a longtrack violent tornado within a simulated. Supercell variations classic and hp and the tornado life. Warm rear flank downdrafts promote tornadoes, while cold rear flank downdrafts discourage them. You should also be able to describe the cloud formation a wall cloud thats often a precursor to a funnel cloud or tornado formation, and identify the location on radar reflectivity where a. Large hail within the rear flank downdraft often shows up brightly as a hook on weather radar images, producing the characteristic hook echo, which often. Direct surface thermodynamic observations within the rear. A strong downdraft of air on the upwind side of a thunderstorm, usually a supercell, which is separated from the forward flank outflow regions of the storm. A condensation funnel is made up of water droplets and extends downward from the base of the thunderstorm. We see in this animation the tornado, the wall cloud with the updraft is, but look that rear flank down draft and. Vorticity increases and the pressure falls mb in 3 hours.
In the radar image above, the rearflank downdraft rfd is where the core of heavy rain and hail is occurring pink pixels, and the forwardflank downdraft ffd is to the east, or right, of the rfd. The rear flank downdraft is the motion in the storm that causes the hook echo feature on radar. Rear flank downdraft or rfd a region of dry air subsiding on the back side of, and wrapping around, a mesocyclone. Secondly, hook echoes form through advection of precipitation. Despite the longsurmised importance of the hook echo and rear. Oct 14, 2010 once a tornado has formed, it follows a predictable life cycle. The rear flank downdraft air tends to be dry and warm since the air warms by adiabatic compression as it sinks to the surface. Once the severe thunderstorms began to form across western oklahoma after 18.
Sep 25, 2017 rear flank downdraft meaning rear flank downdra. Some other complex factors beyond the scope of the course also contribute to the formation of the rfd, but the bottom line is that a separate rear flank downdraft exists in supercells. The inflection point between the rear and forwardflank downdraft boundaries was a focal point for the. The rear flank downdraft or rfd is a region of dry air wrapping around the back of a mesocyclone in a supercell thunderstorm. Secondly, hook echoes form through advection of precipitation from the rear of the main echo around the region of strong updraft.
Rearflank downdrafts have a wellestablished association with hook echoes. Nrot on gr2 radar was going crazy on the backside of the texas storm. Some air, as it collides into the side of a thunderstorm, is pushed down toward the surface. An animation of the simulated cloud and precipitation fields also shows features routinely observed, such as periodic rain curtains that wrap around the lowlevel mesocyclonetornado and a tornado that becomes more rain wrapped in time. Other reliable radar observations have been made that suggest that hook echo formation, in at least some cases, appears to result from the descent of a rain curtain in the rearflank downdraft e. For much of its life cycle, the storm structure of mesovortex 2 was similar to that of a supercell. Compare selected click up to three compare checkboxes for sidebyside product comparisons. Cold air downbursts impinging upon the tornado as it approached davidson county would have caused the tornado funnel to tilt increasingly from the vertical, becoming a funnel cloud as it lifted above the ground and possibly dissipating over davidson. The rfd even comes with its own gust front, as the leading edge of raincooled air. Estimates of rearflank downdraft buoyancy as a predictor of tornadogenesis. Northnortheast of masters and over the riverside reservoir we see a bullseye of high kdp values 3. In warren county, an ef1 tornado packing estimated 90 to 95 mph winds touched down 8 miles south of mcminnville, tennessee, and traveled a path of 3 miles. The rfd even comes with its own gust front, as the leading edge of raincooled air spreads out laterally from the splashdown point of the rfd.
Jun 18, 2017 in the radar image above, the rear flank downdraft rfd is where the core of heavy rain and hail is occurring pink pixels, and the forward flank downdraft ffd is to the east, or right, of the rfd. There are both linear and nonlinear forcings and it is tough to make a general model so often special case scenarios are developed e. Following the development of the rfd, the simulated storm acquires a horseshoeshaped updraft prior to tornadogenesis similar to observations lemon and doswell 1979. It appears in the animation that some extreme winds are pushing out the southwest flank of the supercell with a haze near the cloud edge. Viking rear downdrafts work quietly behind cooktops and rangetops to eliminate smoke and odors, then conveniently hide away when the job is done. Specifically, you should be able to describe the forward flank downdraft, rear flank downdraft, updraft region, mesocyclone, and tornado if applicable. Convective storm structure and evolution eumetrain.
A rear flank downdraft is cold air on the back side of the storm that rushes down towards the ground and when that cold air hits the cloud base associated with the updraft it quickly erodes them leaving a clear slot. Thats the rear flank downdraft and thats the cool air on the backside of the storm that comes crashing around it can help tighten the circle. Other reliable radar observations have been made that suggest that hook echo formation, in at least some cases, appears to result from the descent of a rain curtain in the rear flank downdraft e. Once a tornado has formed, it follows a predictable life cycle. Rear flank downdrafts have a wellestablished association with hook echoes. Perhaps the bestrecognized radar feature in a horizontal depiction associated with supercells is the extension of lowlevel echo on the rightrear flank of these storms, called the hook echo. Mar 03, 2005 vertical pressure gradient fields of supercells get very complex, particularly for nonideal shear profiles. First, the mesocyclone rotating air, along with the rear flank downdraft rfd, starts moving towards the ground. Markowski department of meteorology, the pennsylvania state university, university park, pennsylvania. Markowski department of meteorology, the pennsylvania state university, university park, pennsylvania manuscript received 19 march 2001, in. Jul 25, 2016 time lapse video 8x speed of the tornadic supercell west of syracuse, ks on 71516. The forward flank downdraft is the outflow from the raincooled air of the storms downdraft. Originally a meteorological term, meaning in a supercell thunderstorm, an area of dry air that wraps around the back end of a mesocyclone. The data appear to have resolved a portion of the rear flank downdraft rfd gust front and a portion of the occlusion process.
Rfds mainly occur within classic and hp supercells although rfds have been observed within lp supercells. The above animation shows the evolution of a mesolow on the southwest flank of a supercelllike thunderstorm, which becomes the new surface low pressure. The storm had a persistent mesovortex similar to a mesocyclone, and it developed a hook echo, inflow notch, and a reflectivity core. Labels show rear flank downdraft descent, counterrotating vortices, and storm inflow. Mesovortices and their interactions within a quasilinear.
It often is visible as a clear slot wrapping around the wall cloud rfd rear flank downdraft. Early april east coast cyclone satellite liaison blog. Super tornado cadens visualization enabling discovery. The combination of these parameters suggests the presence of large hail in this region of the rear flank downdraft. Derived from data, blue streamers falling toward the ground indicate the tornados rear flank downdraft, while the quickly rising orange lines constitute the updraft. At such close distance to the radar modelengineering les method was used to analyze a tornado and nearground turbulence under realistic conditions. The rear flank downdraft of a supercell is a very complex and not yet fully understood feature. Large hail within the rear flank downdraft shows up brightly as a hook on weather radar images, producing the characteristic hook echo, which indicates the.
Here is a short clip from 15km north of dubbo where textbook rfd rear flank downdraft winds are being heard and observed. Multiple circulations attempt to develop on the rfdinflow interface before the entire area is undercut by outflow from the storms forwardflank. Supercell rearflank downdraft rfd surge capron, ok, may 8. Streamtubes are driven by a wind field parameter in a computational scientific model of the deadly 2011 joplin, missouri tornado. Estimates of rear flank downdraft buoyancy as a predictor of tornadogenesis. Specifically, you should be able to describe the forwardflank downdraft, rear flank downdraft, updraft region, mesocyclone, and tornado if applicable.
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